Burlington County's drinking water often comes from wells tapping into aquifer 121CKKD, where groundwater flows through layers of rock and soil before reaching home taps. The hardness in this water, mainly from calcium and magnesium dissolved from natural sources, varies across the area. Local sampling by the U.S. Geological Survey from 2010 to 2024 reveals a broad range of hardness results but no federal safety thresholds are exceeded.
What happens when hard water remains untreated for years in a household?
When hardness minerals like calcium and magnesium are not addressed, scale buildup can occur in pipes, fixtures, and appliances. This buildup often leads to reduced water flow and efficiency, increased maintenance needs, and potential damage to water-using appliances over time. Though hard water is not a health hazard, the accumulation can affect water heating performance and appliance lifespan.
What do 'detected', 'median', and 'range' mean in the Burlington County water hardness data?
In the sampled wells from aquifer 121CKKD, hardness was detected in 35 out of 37 results, indicating the presence of calcium and magnesium ions at measurable levels. The term 'median' refers to the middle value in the dataset—3.19 mg/L hardness—showing a central tendency of the area’s groundwater hardness. The 'range' spans from the lowest detected value of 0.65 mg/L to the highest at 136.0 mg/L, highlighting variability depending on well depth and local geology. Importantly, none of these figures exceed federal health thresholds, meaning hardness levels pose no regulatory safety concerns.
How should you judge salt-free water softening treatment capacity against your household’s daily water demand?
Water treatment capacity should align with the total water volume your household uses each day. To evaluate this capacity, measure your average water consumption—usually in gallons per day—and compare it with the capabilities of any salt-free softening system you consider. Ensuring the system can manage your usage without frequent regeneration or loss of performance helps maintain effective scale control. Household size, appliance water use, and peak water use times all influence this assessment.
How can a Burlington County homeowner interpret the hardness median and range in aquifer 121CKKD?
For a homeowner relying on the local aquifer, the median hardness of 3.19 mg/L reflects typical groundwater hardness but doesn’t predict individual well conditions. The wide range up to 136.0 mg/L means some wells have much higher hardness. This variation highlights the importance of conducting a specific water test for your well, as local conditions may differ significantly from the median. Knowing your well’s exact hardness enables a better choice between treatment options.
What household symptoms indicate untreated water hardness, and which do not?
Common signs of untreated hardness include mineral spots on dishes and fixtures, scaling inside appliances like water heaters, and reduced water heater efficiency. These symptoms arise from calcium and magnesium minerals depositing over time. However, discoloration, unpleasant tastes or odors, or health-related symptoms are not direct indicators of hardness and should prompt separate water quality testing. Recognizing the difference helps target treatment efforts properly.
To confirm whether salt-free water softening is the right approach for your Burlington County home, order a water hardness test specific to your well. This analysis will determine the calcium and magnesium concentrations directly affecting your household water. A result showing hardness within the local range but closer to the higher end would support considering a Pentair Salt-Free Scale Control System, which is designed to reduce scaling effects without adding salt. This targeted test is the essential step for making a well-informed decision on water treatment.
Where this information comes from
Source: USGS groundwater sampling. Sampled 2024-06-05. These figures describe groundwater sampled in this area. They are not a test of any individual private well - only a test of that well can establish its own water.
On record: U.S. Geological Survey sampling of Hardness, Ca, Mg in the 121CKKD aquifer (Burlington County): 37 results from 13 wells, median 3.19 mg/L, range 0.65-136.0 mg/L; none above any federal threshold
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